Monitoring One Of The Tipping Points Of The Amoc

Abstract The deep limb of the AMOC is fed by two main sources: a western source generated by deep convection in the Labrador/Irminger seas, and an eastern source originating in overflow of dense water from the Nordic Seas across the Greenland-Scotland Ridge, which is enhanced by water entrained afte...

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Bibliographic Details
Main Authors: Larsen, Karin Margretha H., Hansen, Bogi, Østerhus, Svein
Format: Still Image
Language:English
Published: Zenodo 2018
Subjects:
AMOC
Tipping point
Monitoring
Greenland-Scotland Ridge
Faroe Bank
Greenland
Nordic Seas
Online Access:https://dx.doi.org/10.5281/zenodo.1188870
https://zenodo.org/record/1188870

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